首页> 外文期刊>Geostandards and geoanalytical research >Simultaneous Determination of Fluorine, Chlorine, Bromine and Iodine in Six Geochemical Reference Materials Using Pyrohydrolysis, Ion Chromatography and Inductively Coupled Plasma-Mass Spectrometry
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Simultaneous Determination of Fluorine, Chlorine, Bromine and Iodine in Six Geochemical Reference Materials Using Pyrohydrolysis, Ion Chromatography and Inductively Coupled Plasma-Mass Spectrometry

机译:热解,离子色谱和电感耦合等离子体质谱法同时测定六种地球化学参考物质中的氟,氯,溴和碘

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Concentrations of halogens (fluorine, chlorine, bromine and iodine) were determined in six geochemical reference materials (BHVO-2, GS-N, JG-1, JR-1, JB-1b, JB-2). Halogens were first extracted from powdered samples using a pyrohydrolysis technique, then hydrolysis solutions were analysed by ion chromatography for F and Cl and inductively coupled plasma-mass spectrometry for Br and I. The detection limits in solutions were 100 μg l-1 for both F and Cl and 10 ng l-1 for Br and I. Considering the extraction procedure, performed on a maximum of 500 mg of sample and producing 100 ml of pyrohydrolysis solution, detection limits in rock samples were 20 mg kg-1 for F and Cl and 2 μg kg-1 for Br and I. The mean analytical errors on the studied composition ranges were estimated at 10 mg kg-1 for F and Cl, 100 μg kg-1 for Br and 25 μg kg-1 for I. The concentration values, based on repeated (generally > 10) sample analysis, were in good agreement generally with published values and narrowed the mean dispersion around mean values. Large dispersions are discussed in terms of samples heterogeneity and contaminations during sample preparation. Basaltic RMs were found to be more suitable for studies of halogen compositions than differentiated rock material, especially granites – the powders of which were heterogeneous in halogens at the 500 mg level.
机译:在六种地球化学参考材料(BHVO-2,GS-N,JG-1,JR-1,JB-1b,JB-2)中测定了卤素(氟,氯,溴和碘)的浓度。首先使用热水解技术从粉末状样品中提取卤素,然后通过离子色谱法分析F和Cl的水解溶液,然后通过电感耦合等离子体质谱法分析Br和I的溶液。F的检测限均为100μgl-1对于Cl和Cl,Br和I为10 ng l-1。考虑到萃取程序,最多可提取500 mg样品并产生100 ml热解溶液,岩石样品中F和Cl的检出限为20 mg kg-1对于Br和I为2μgkg-1。对于所研究的组成范围,平均分析误差估计为F和Cl为10 mg kg-1,Br为100μgkg-1和I为25μgkg-1。基于重复(通常> 10)样本分析的浓度值通常与已公布的值高度吻合,并且使平均分散范围缩小到平均值附近。就样品制备过程中的样品异质性和污染而言,讨论了较大的分散体。发现玄武质RMs比分化的岩石材料(尤其是花岗岩)更适合研究卤素成分,而花岗岩的粉末在卤素含量为500 mg时是非均质的。

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